地表破裂,surface rupture英语短句,例句大全

地表破裂,surface rupture
1)surface rupture地表破裂
1.The basic characteristics of near-fault ground motion,including the concentration of near-fault strong ground motions,the surface rupture and fling-step,the rupture directivity effect,the near fault large velocity pulse and the hanging wall effect,are discussed in this paper.本文对近断层地震动的基本特征作了详细分析,这些基本特征主要包括近断层强地震动的集中性、地表破裂、地面永久变形、破裂的方向性效应、近断层速度大脉冲和上盘效应。
2.Field investigation on the surface ruptures of the MS8.0地震地表破裂的野外地质调查表明,在这一段内主要存在一条地震地表破裂带,总体沿北川-青川断裂带分布。
3.By laying emphasis on the geomorphic features of the surface ruptures of the huge earthquake in Longmen Mountains on the eastern margin of Qinghai-Tibet Plateau,this paper confirms the vertical and horizontal offsets of the Yingxiu-Beichuan fault and the Pengxian-Guanxian fault by detailed field geomorphic surveys.作者以地表破裂为切入点,在映秀-北川断裂和彭灌断裂的关键部位,对断错山脊、洪积扇、河流阶地、边坡脊、断层陡坎、河道错断、冲沟侧缘壁位错、小路位错、公路位错、公路拱曲、构造裂缝、断层偏转、擦痕、挤压脊、坡中槽等汶川地震所导致的地表破裂和断裂带开展了详细的野外地貌测量,标定了映秀-北川断裂带和彭灌断裂的垂向断距和水平断距,结果表明汶川地震的地表破裂带沿北东东向延伸,走向介于NE30°~50°之间,倾向北西,倾角介于30°~40°之间。

英文短句/例句

1.Characteristics of the Surface Rupture of the M_S8.0 Wenchuan Earthquake on the Epicenter,Yingxiu Area汶川地震震中映秀地区地表破裂特征
2.A New Discoved Co-seismic Surface Rupture Zone on Changlingshan Northern Piedmont Fault长岭山北麓断裂上新发现的地震地表破裂带
3.The Surface Rupture of the M_S8.0 Wenchuan Earthquake on the Northern Segment of Central Fault汶川M_S8.0地震中央断裂北段地表破裂特征
4.Surface Ruptures Induced by Associated Wenchuan Earthquake in Yingxiu and Hongkou Area汶川大地震中映秀-虹口地区的地表破裂
5.The Survey of Geological Condition and Surface Rupture Characters of Yingxiu Town in the Wenchuan Earthquake汶川地震映秀镇地质条件与地表破裂特征调查
6.Geometry and kinematics in the east segment of the surface rupture zone occurring during the Kunlun earthquake昆仑山地震地表破裂带东段几何学与运动学
7.Setback distance determination in reconstruction along the trace of surface rupture caused by M_s8.0 Wenchuan earthquake汶川地震地表破裂周围建筑物重建的避让距离
8.Deformation Features of Surface Rupture of the Wenchuan Earthquake (M8.0) at the Bailu Town汶川8.0级地震地表破裂白鹿镇段的变形特征
9.DISCOVERY OF SURFACE RUPTURE ZONE ON THE SOUTH OF HELISHAN IN GAOTAI,GANSU PROVINCE甘肃高台合黎山南缘发现地震地表破裂带
10.DEFORMATION STYLES OF THE NORTHERNMOST SURFACE RUPTURE ZONE OF THE M_S 8.0 WENCHUAN EARTHQUAKE汶川M_S 8.0地震地表破裂带北端位置的修订
11.Surface Rupture Features and Segmentation of the M_S8.0 Wenchuan Earthquake汶川8级大地震的地表破裂特征及分段
12.GEOLOGICAL BACKGROUND OF LONGMEN SHAN SEISMIC BELT AND SURFACE RUPTURES IN WENCHUAN EARTHQUAKE龙门山地震带的地质背景与汶川地震的地表破裂
13.CHARACTERISTICS OF SURFACE RUPTURE OF EL ASNAM (ALGERIA) EARTTHQUAKE AND THE STUDY OF PALEOSEISMIC EVENTS阿尔及利亚阿斯南地震地表破裂特征及古地震事件研究
14.Conditions for earthquake surface rupture along the San Andreas fault system, California沿加利福尼亚圣安德烈斯断层系地震引起地表破裂的条件
15.Research of Distribution Feature of Strain Field and Evolution of Surface Rupture Caused by Earthquake Fault;地震断层错动产生的应变场特征的研究及地表破裂的评价
16.Characteristics of Ground Ruptures in Beichuan County Caused by the Wenchuan Earthquake汶川地震北川县城地表断层破裂特征
17.The actual cause of the quake itself is the rupturing or breaking of rocks at or below the earth's surface.地震本身的真正原因是地球表面的或地底下的岩石断裂或破裂。
18.She'll break up bit by bit.她（船）会一块一块地破裂。

相关短句/例句

surface rupture zone地表破裂带
1.From north to south,most of the widths of intense surface rupture zones are less than 40m,and above 1/2 are between 10～30m.0级地震地表破裂带的实地调查,龙门山断裂带的中央断裂与前山断裂地表破裂带宽度自北向南一般<40m。
2.Based on the latest displacement of Huoshan piedmont fault,Mianshan west-side fault and Taigu fault obtained from the beginning of 1990′s up to the present,the characteristics of distribution and displacement of surface rupture zone of the 1303 Hongtong M =8 earthquake,Shanxi Province are synthesized and discussed in the paper.综合 2 0世纪 90年代初在霍山山前断裂和近年在绵山西侧断裂和太谷断裂获取的最新调查资料 ,讨论了 130 3年山西洪洞 8级地震地表破裂带的展布和位移特征。
3.To know the shallow geological structures under the surface rupture zone,a high-resolut.此项探测研究以出现在什邡市师古镇附近的疑似地震地表破裂带为切入点,通过采用可控震源以及高精度的浅层地震反射勘探方法,获得了深度15～800m范围内高分辨率的地下结构和构造图像。
3)surface rupture地表破裂带
1.Its surface rupture occurs on the Beichuan-Yingxiu and the Jiangyou-Guanxian faults,with the lengths of 200km and 70km,respectively.地表破裂带的最大挤压缩短量为3。
2.Besides the huge casualties and property losses, a most complicated yet longest thrust-type co-seismic surface rupture zone was developed in the quake-hit area.0),地震不仅造成巨大的人员伤亡和财产损失,并形成了迄今为止空间上分布最为复杂、长度最大的逆冲型同震地表破裂带。
4)earthquake surface rupture地震地表破裂
5)seismic surface deformation地震地表破裂带
1.Primary study on seismic surface deformation and faulting behavior of Central Fault (Beichuan-Yingxiu Fault) is done by methods such as topographic analysis, field geological investigation, trench excavation, geological profile analysis and so on.目前对其活动速率、活动性、强震复发周期以及震后其地震地表破裂带特征等重要的科学问题上都还没有统一的认识。
6)surface rupture distribution地表破裂分布图